11,053 foot Mammoth Mountain Ski area in winter and mountain bike park in summer |
Besides our wonderful day trip to the
Ancient Bristlecone Forest we enjoyed a few other excursions during our short
stay in Mammoth Lakes. This area of the
Sierra Nevada is not only rich with alpine scenery but geologic wonders as
well. Evidence of glaciation and both
ancient and recent volcanic activity are scattered all over the place. We visited an earthquake fissure, two volcanic
explosion pits which contain small lakes, the dormant volcanic peak of Mammoth
Mountain plus a ‘pile’ of lava columns better known as the Devils Postpile
National Monument.
One of the Inyo Craters, formed by volcanic explosions |
The Devils Postpile National Monument |
The Devils Postpile is a remarkable
geological feature of tall, vertical columns formed by a flow of basaltic lava. As the molten lava cooled and contracted to
solid rock, cracks formed at 120-degree angles to absorb the stress. Cracks merged with other cracks and created
the hexagonal columns.
Some columns have been twisted and distorted |
We hiked around the monument marveling at the huge columns. There is a trail to the top of the "pile" where the surface of the columns have been polished smooth by glaciers. So the side view is one of tall pillars of rock and the top view looks like hexagonal paving stones. Amazing... Nature uses the hexagon shape in many things - bee hives, soap bubbles, salt flats and turtle shells.
The top of the 'pile' looks like paving stones Notice the parallel grooves or glacial striations carved in the rock by moving glaciers |
From the Devil's Postpile, we took the trail along the San Joaquin River to Rainbow Falls. The falls is formed by a lava ledge. The San Joaquin River plunges down this ledge 101 feet into a deep gorge. Rainbow colors form in the mists below the falls.
Rainbow Falls |
Mono Lake with tufa formations near shore Tufa is formed by the mineral deposits of once flowing springs |
Mono Lake is an excellent example of how America’s
view of the environment and of using land and water has changed for the
better. Since the 1960’s the city of Los
Angeles diverted the fresh water streams that flowed into Mono Lake for its own
use. At the time, most likely the
thinking was that a salt lake didn’t need fresh water flowing into it and the
people of Los Angeles did need fresh water.
(Why Los Angeles thought it had a right to water more than 350 miles
away that never flowed toward the city is a whole other matter, but I won’t
even go there.)
Mono Lake is two-and-a half times as salty
as seawater and maybe that made it seem too inhospitable to support much life
and thus okay to take the fresh water away.
But the water of Mono Lake teems with life! Brine shrimp and alkali fly larvae attract
millions of migrating birds and many California Seagulls use the lake for
nesting grounds and to feed their young.
More tufa formations in the lake |
Over the years as more and more water was
diverted from Mono Lake, the water levels dropped and the chemistry of the lake
changed threatening the shrimp and fly larvae and the birds that depended on
this food source. What was once a
healthy ecosystem was in real danger of disappearance. Many people and organizations advocated for
protective action for Mono Lake. And to
make a long story short, a compromise was reached in 1994 to return the lake’s
level to 6392 feet, twenty feet higher than the historic low.
Believe it or not, we didn't see everything in the Mammoth Lakes area. But we needed to move on so we could spend several
days in the Ansel Adams Wilderness and hike on the Pacific Crest Trail. Even when you have all the time you want,
there still isn’t enough time to see and do everything. Maybe next time?
Days Hiked 3
Total Miles Hiked 8.69
Ave. Miles per Day 2.90
Total Elevation Gain 1,225
Ave. Elevation Gain per day 411
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